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B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza Basics of groundwater hydrology  and geotechnical engineering Prepared by Dr O. Hamza o_hamza   at  hotmail   dot  com Lecture reference: OH_GA01
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Content  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
Basic groundwater hydrology Hydrologic Cycle B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
Basic groundwater hydrology Subsurface water occurs in two different zones: saturated and unsaturated Hydrologic Cycle B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 Saturated zone Unsaturated zone
Basic forms of geotechnical structure  Study of groundwater is essential for engineers who construct dams, tunnels, water conveyance channels, mines, and other structures.  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 Natural slope Cut slope Embankment dam Building foundation Supported excavation Tunnel Road embankment Construction on soft soil Offshore foundation
Basic problems in geotechnical engineering  Water may contribute to both types of problem. Therefore, successful designing requires adequate consideration of groundwater effects.  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Basic mechanics of soil  Analysis of stress and strain   Stresses Strains What is stress and strain? Why the relation between stress and strain is so important? B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 Loads on soil Instability & Settlements
Basic mechanics of soil  Analysis of stress and strain   Stresses and strains occur in all directions and to do settlement and stability analyses it is often necessary to relate the stresses in a particular direction to those in other directions.  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 stress strain mean p' = (s' a  + 2s' r ) / 3 s' = (s' a  + s' r ) / 2 e v  = DV/V = (e a  + 2e r ) e n  = (e a  + e r ) deviator q' = (s' a  - s' r ) t' =  (s' a  - s' r ) / 2 e s  = 2 (e a  - e r ) / 3 e g  = (e a  - e r )
Basic mechanics of soil  Analysis of stress and strain   To  visualise  the stresses on all the possible planes, a graph called the  Mohr circle  is drawn by plotting a (normal stress, shear stress) point for a plane at every possible angle.   Mohr circle B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza Uniaxial compression Uniaxial extension   Shearing GA01
Basic mechanics of soil  Analysis of stress and strain   Do you think of any material parameter? Stress-strain relation, stiffness and strength   B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 Stresses Strains Constitutive law Material properties/ parameters Stiffness parameters Strength parameters Change of size: bulk modulus  K Change of shape: shear modulus  G Change of 1-dimension:  Young’s modulus  E
Basic mechanics of soil  Rigid mechanics   When soils fail they develop distinct  slip surfaces Analysis of stress and strain   B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 retaining wall Soil
Equilibrium  is examined by construction of a polygon of forces.   Basic mechanics of soil  Rigid mechanics   Similarly  Compatibility of displacements  is examined by construction of a displacement diagram   Slip surfaces divided soil or rock into blocks, so the principles of rigid body mechanics can be applicable  . Analysis of stress and strain   B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
Basic mechanics of soil  Special stress and strain states   ,[object Object],[object Object],[object Object],B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 The state of stress in the ground is complex.
Basic mechanics of soil  Special stress and strain states   Isotropic:   Equal stress in radial direction. Applicable to triaxial test before shearing.  p' = (  ' a  + 2  ' r ) / 3  = mean stress   v  =   V / V o   = volumetric strain  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
One-dimensional:   Horizontal strains are zero. Applicable to oedometer test and in the ground below  wide  foundations, embankments and excavations.   ' z  = vertical stress   v  =   V / V o  = volumetric strain Basic mechanics of soil  Special stress and strain states   GA01 B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza where e 0  is the initial void ratio (before stress increment)
Summary  ,[object Object],[object Object],[object Object],[object Object],[object Object],B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
Example problems  Problem 1   The figure shows a rigid triangular block of soil with a slip surface. Two of the forces, acting on the block, are known to be W=160kN and T=60kN. Determine the value of P to ensure the equilibrium of the block.  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 45 o
Example problems  Consider a suitable scale e.g. 1cm=20kN Problem 1   The figure shows a rigid triangular block of soil with a slip surface. Two of the forces, acting on the block, are known to be W=160kN and T=60kN. Determine the value of P to ensure the equilibrium of the block.  B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01 45 o
Example problems  Problem 2   An element of soil behind a retaining wall; the effective vertical and horizontal stresses are   z =300kPa and   h =100kPa and these are principal stresses. Draw Mohr's stress circle and determine the maximum shear stress. B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza
Example problems  Problem 2   An element of soil behind a retaining wall; the effective vertical and horizontal stresses are   z =300kPa and   h =100kPa and these are principal stresses. Draw Mohr's stress circle and determine the maximum shear stress. B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01  max
Example problems  Problem 3   At the beginning of odeometer test, the void ratio and thickness of the specimen was 0.891 and 19mm respectively. Find the final void ratio e f  if the soil consolidated by 3.52mm (i.e.   H). B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
Example problems  Problem 3   At the beginning of odeometer test, the void ratio and thickness of the specimen was 0.891 and 19mm respectively. Find the final void ratio e f  if the soil consolidated by 3.52mm (i.e.   H). Void ratio change =   e = e o  – e f   We have   H=3.52mm, initial void ratio e 0 =0.891 and initial thickness H0=0.891mm Thus,  the final void ratio of the soil e f  =0.54 B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01
B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza ,[object Object],[object Object],[object Object],References ,[object Object],[object Object],GA01
End of Unit B asics of groundwater hydrology and geotechnical engineering  Dr. O Hamza GA01

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Basics of groundwater hydrology in geotechnical engineering oh ga01

  • 1. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza Basics of groundwater hydrology and geotechnical engineering Prepared by Dr O. Hamza o_hamza at hotmail dot com Lecture reference: OH_GA01
  • 2.
  • 3. Basic groundwater hydrology Hydrologic Cycle B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01
  • 4. Basic groundwater hydrology Subsurface water occurs in two different zones: saturated and unsaturated Hydrologic Cycle B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 Saturated zone Unsaturated zone
  • 5. Basic forms of geotechnical structure Study of groundwater is essential for engineers who construct dams, tunnels, water conveyance channels, mines, and other structures. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 Natural slope Cut slope Embankment dam Building foundation Supported excavation Tunnel Road embankment Construction on soft soil Offshore foundation
  • 6.
  • 7. Basic mechanics of soil Analysis of stress and strain Stresses Strains What is stress and strain? Why the relation between stress and strain is so important? B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 Loads on soil Instability & Settlements
  • 8. Basic mechanics of soil Analysis of stress and strain Stresses and strains occur in all directions and to do settlement and stability analyses it is often necessary to relate the stresses in a particular direction to those in other directions. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 stress strain mean p' = (s' a + 2s' r ) / 3 s' = (s' a + s' r ) / 2 e v = DV/V = (e a + 2e r ) e n = (e a + e r ) deviator q' = (s' a - s' r ) t' =  (s' a - s' r ) / 2 e s = 2 (e a - e r ) / 3 e g = (e a - e r )
  • 9. Basic mechanics of soil Analysis of stress and strain To visualise the stresses on all the possible planes, a graph called the Mohr circle is drawn by plotting a (normal stress, shear stress) point for a plane at every possible angle. Mohr circle B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza Uniaxial compression Uniaxial extension Shearing GA01
  • 10. Basic mechanics of soil Analysis of stress and strain Do you think of any material parameter? Stress-strain relation, stiffness and strength B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 Stresses Strains Constitutive law Material properties/ parameters Stiffness parameters Strength parameters Change of size: bulk modulus K Change of shape: shear modulus G Change of 1-dimension: Young’s modulus E
  • 11. Basic mechanics of soil Rigid mechanics When soils fail they develop distinct slip surfaces Analysis of stress and strain B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 retaining wall Soil
  • 12. Equilibrium is examined by construction of a polygon of forces. Basic mechanics of soil Rigid mechanics Similarly Compatibility of displacements is examined by construction of a displacement diagram Slip surfaces divided soil or rock into blocks, so the principles of rigid body mechanics can be applicable . Analysis of stress and strain B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01
  • 13.
  • 14. Basic mechanics of soil Special stress and strain states Isotropic: Equal stress in radial direction. Applicable to triaxial test before shearing. p' = (  ' a + 2  ' r ) / 3 = mean stress  v =  V / V o = volumetric strain B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01
  • 15. One-dimensional: Horizontal strains are zero. Applicable to oedometer test and in the ground below wide foundations, embankments and excavations.  ' z = vertical stress  v =  V / V o = volumetric strain Basic mechanics of soil Special stress and strain states GA01 B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza where e 0 is the initial void ratio (before stress increment)
  • 16.
  • 17. Example problems Problem 1 The figure shows a rigid triangular block of soil with a slip surface. Two of the forces, acting on the block, are known to be W=160kN and T=60kN. Determine the value of P to ensure the equilibrium of the block. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 45 o
  • 18. Example problems Consider a suitable scale e.g. 1cm=20kN Problem 1 The figure shows a rigid triangular block of soil with a slip surface. Two of the forces, acting on the block, are known to be W=160kN and T=60kN. Determine the value of P to ensure the equilibrium of the block. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01 45 o
  • 19. Example problems Problem 2 An element of soil behind a retaining wall; the effective vertical and horizontal stresses are  z =300kPa and  h =100kPa and these are principal stresses. Draw Mohr's stress circle and determine the maximum shear stress. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza
  • 20. Example problems Problem 2 An element of soil behind a retaining wall; the effective vertical and horizontal stresses are  z =300kPa and  h =100kPa and these are principal stresses. Draw Mohr's stress circle and determine the maximum shear stress. B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01  max
  • 21. Example problems Problem 3 At the beginning of odeometer test, the void ratio and thickness of the specimen was 0.891 and 19mm respectively. Find the final void ratio e f if the soil consolidated by 3.52mm (i.e.  H). B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01
  • 22. Example problems Problem 3 At the beginning of odeometer test, the void ratio and thickness of the specimen was 0.891 and 19mm respectively. Find the final void ratio e f if the soil consolidated by 3.52mm (i.e.  H). Void ratio change =  e = e o – e f We have  H=3.52mm, initial void ratio e 0 =0.891 and initial thickness H0=0.891mm Thus, the final void ratio of the soil e f =0.54 B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01
  • 23.
  • 24. End of Unit B asics of groundwater hydrology and geotechnical engineering Dr. O Hamza GA01

Notes de l'éditeur

  1. Each one 5-7 minuts